Despite that record, the January, 2010 snow blitz isn't really remembered as a top tier historic snowstorm, like the famous Blizzard of 1888, December, 1969, the Valentine's Blizzard of 2007 or even the Pi Day Blizzard of March, 2017.
The storm 15 years ago is a great illustration of how quirky Vermont weather can be.
The January, 2010, was, oddly, pretty much just a phenomenon of the Burlington area, and not particularly widespread. There wasn't a lot of wind with the storm, and the snow's consistency was like the lightest of feathers.
Usually during winter storms, Burlington receives less snow than the mountains, which can more easily collect moisture, or southern Vermont, which more frequently gets clipped by powerful nor'easters along the coast.
In January, 2010, Burlington got more snow than anyone in Vermont. Nearby Essex Junction was close, with 30 inches, and Charlotte had two feet.
But many other areas of Vermont had just a run of the mill midwinter snowfall. The summit of Mount Mansfield only managed 11 inches. Stowe had just 4.5 inches, and Marshfield had a whopping 2.7 inches.
Snow accumulation of over 20 inches was limited to just most of Chittenden County and northern Addison County. Parts of the Northeast Kingdom and some towns in Rutland and Franklin counties sw a foot or so of snow, but much of central Vermont had six inches or less.
There were two main reasons why the January, 2010 storm hit Burlington so hard but wasn't a big deal elsewhere in the state.
One reason was lake effect. All day, the wind flow was just perfect over the unfrozen Lake Champlain to scoop up moisture into clouds and snow. The other reason was a temperature inversion just about summit level along the Green Mountains.
Usually, the moisture in a northwest wind flow doesn't release snow until the wind is forced to ride up the west slopes of the Greens. In January, 2010, that inversion blocked the air flow, so the snow was released from the clouds over Chittenden County, and not the mountains to the east.
OTHER STORMS
Other historic snowstorms in Vermont hit much wider areas, which of course made them more memorable. The Valentine's Day blizzard in 2007 deposited 20 to 30 inches snow on almost all of the state.
The Pi Day Blizzard spread 20 to 35 inches of snow across most of central and northern Vermont along with most of New York and parts of Pennsylvania.
Another reason why the January, 2010 storm was so manageable was the lack of water in the snow. It was so light and fluffy that you can almost clear it away with a leaf blower. If you melted Burlington's big January, 2010 storm down, you get the equivalent of just under an inch of rain.
Fluffy snow packs down more readily, too. So within days of the big storm, there wasn't all that much snow on the ground. Despite continuously below freezing temperatures and 9.1 inches of additional snow in the interim, the snow depth in Burlington was down to 13 inches by January 13.
The snow pretty much went away on its own.
Other big snowstorms in Burlington had a much higher water content, meaning the snow was heavier. That made the snow harder to shovel, harder to plow, and easier to get stuck in. Plus, the only way to get rid of the dense snow was through thawing.
Despite temperatures in the single digits above zero, the snow in the Valentine's blizzard of 2007 was dense and heavy. The 25.7 inches of snow that fell in that storm consisted of just under two inches of water.
Another heavy snowstorm in March, 2011 - now Burlington's fourth largest with 25.8 inches, had a storm total of 2.43 inches of liquid, though the first few hours of that storm was in the form of rain, not snow.
On December, 25-28, 1969, Burlington was hit by 29.7 inches of snow. The water equivalent was 2.73 inches.
The Pi Day Blizzard in March, 2017 was also relatively light and fluffy, but not quite as feathery as January, 2010. Pi Day dumped 30.4 inches of snow on Burlington with a water equivalent of 1.13 inches.
So yes, the January, 2010 snowstorm was a big deal, at least for Burlington. But what makes a snowstorm truly memorable is not just the amount, but the consistency of the snow, the wind, and how widespread the storm is.